Abstract

Abstract Following the discovery of the first exoplanet candidate transiting a white dwarf (WD), a “white dwarf opportunity” for characterizing the atmospheres of terrestrial exoplanets around WDs is emerging. Large planet-to-star size ratios and hence large transit depths make transiting WD exoplanets favorable targets for transmission spectroscopy; conclusive detection of spectral features on an Earth-like planet transiting a close-by WD can be achieved within a medium James Webb Space Telescope program. Despite the apparently promising opportunity, however, the post-main sequence evolutionary history of a first-generation WD exoplanet has never been incorporated in atmospheric modeling. Furthermore, second-generation planets formed in WD debris disks have never been studied from a photochemical perspective. We demonstrate that transmission spectroscopy can identify a second-generation rocky WD exoplanet with a thick (∼1 bar) H2-dominated atmosphere. In addition, we can infer outgassing activities of a WD exoplanet based on its transmission spectra and test photochemical runaway by studying CH4 buildup.

Highlights

  • An exciting opportunity for characterizing the atmospheres of terrestrial exoplanets transiting white dwarf (WD) is emerging

  • Large planet-to-star size ratios and large transit depths make transiting WD exoplanets favorable targets for transmission spectroscopy – conclusive detection of spectral features on an Earthlike planet transiting a close-by WD can be achieved within a medium James Webb Space Telescope (JWST) program

  • The key difference between these two high mean molecular weight (MMW) atmospheric compositions and the H2-dominated scenario is that a WD exoplanet with a high MMW atmosphere can either be first- or second-generation

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Summary

Introduction

An exciting opportunity for characterizing the atmospheres of terrestrial exoplanets transiting WDs is emerging. Kaltenegger, MacDonald et al (2020) explored the possibility of observing transiting Earth-like WD planets with JWST and described a “white dwarf opportunity” of detecting biosignature gases on such planets. For a hypothetical Earthsized planet with Earth-like atmosphere transiting WD 1856+534, JWST can detect H2O and CO2 with just a few transits and detect biosignature gases such as the O3 + CH4 pair in 25 transits (Kaltenegger, MacDonald et al 2020). JWST would struggle to detect the O3 + CH4 biosignature pair on a terrestrial planet orbiting a M dwarf such as TRAPPIST-1e even with 100 transits (e.g., Lin et al 2021)

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